The answer is both simple and complex.
The lava from below pushes up from underground. The rim of the hole becomes coated with cooled lava. as this process continues the rim gets higher and higher.
It gets smaller towards the top as a result of simple gravitational dynamics.
The particles that would make the cone a cylinder fall away and never become a permanent part of the wall.
In addition as it grows plugs form; which allow the outside to harden even more resisting the internal pressure to bulge.
Most of the lava which exits the volcano tends to gather at the lowest level outside the cone, which also makes the base wider.
Why are some volcanoes cone shaped?
The rim of the hole becomes coated with cooled lava. as this process continues the rim gets higher and higher.
Volcanoes are usually cone shaped mountains or hills.
Most types of volcanoes are either crater shaped or cone shaped. Stratovolcanoes are shaped like tall cone mountains and shield volcanoes are more flat and spread out.
volcanoes
Very tall volcanoes with sharp peaks are stratovolcanoes.
Mount Taal is a cinder cone volcano because it has a bowl shaped crater.
Volcanoes are cone shaped.
Composite Volcanoes!
Volcanoes are usually cone shaped mountains or hills.
Composite Volcanoes!
yes
Most types of volcanoes are either crater shaped or cone shaped. Stratovolcanoes are shaped like tall cone mountains and shield volcanoes are more flat and spread out.
volcanoes
volcanoes
Very tall volcanoes with sharp peaks are stratovolcanoes.
They are shield volcanoes. This means that they are cone shaped but with very shallow slope angles forming the volcanoes flank.
Mount Taal is a cinder cone volcano because it has a bowl shaped crater.
volcanoes in guatemala